Followed by "Introduction to Academicians of the Department of Geosciences of the Chinese Academy of Sciences (12)" (in alphabetical order of surname).
Xiao Wenjiao, male, Han nationality, born in Lianyuan, Hunan Province in December 1967, is an academician of the Chinese Academy of Sciences, a researcher of the Xinjiang Institute of Ecology and Geography of the Chinese Academy of Sciences, the president of the Xinjiang Branch of the Chinese Academy of Sciences, and an academician of the European Academy of Sciences. Member of the 14th National Committee of the Chinese People's Political Consultative Conference.
Xiao Wenjiao graduated from the Department of Geology of Changchun Institute of Geology in 1989In 1992, he obtained a master's degree from the Graduate School of China University of Geosciences (Beijing).In 1995, he received his Ph.D. from the Institute of Geology, Chinese Academy of Sciences, and then joined the Institute of Geophysics, Chinese Academy of SciencesIn 1997, he worked in the Open Laboratory of Lithospheric Tectonic Evolution, Institute of Geology, Chinese Academy of SciencesIn 1998, he joined the Institute of Geology and Geophysics, Chinese Academy of Sciences, and successively served as associate researcher and researcherIn 2007, he was awarded the National Science Grant for Distinguished Young ScholarsFrom 2011 to 2020, he served as the deputy director of the Xinjiang Institute of Ecology and Geography, Chinese Academy of SciencesIn 2019, he was elected as an academician of the Chinese Academy of SciencesIn 2020, he served as the President of the Xinjiang Branch of the Chinese Academy of Sciences.
Xiao Wenjiao is mainly engaged in the study of orogenic and metallogenesis in the Tethys and Central Asian orogenic belts, and his research interests include: plate tectonics, structural geology, ophiolite, accretionary wedges, sedimentary basins, Central Asian accretionary orogeny and mineralization, and the evolution of the Tethys orogenic belt. Through field anatomy and chronological work, he determined the complex active continental margin system and its attributes, tectonic styles and formation ages in the West Kunlun Orogenic Belt, determined the magmatic arcs and accretionary cuneiform rocks superimposed on the Early Paleozoic collage, and the characteristics of the early Paleozoic-Early Mesozoic southward composite accretional orogenyThis paper systematically analyzes the temporal and spatial distribution characteristics of arc-related active continental margin components in the Central Asian orogenic belt, obtains Cambrian Paleo-Asian oceanic chronological evidence, proposes that the southern margin of Siberia undergoes multidirectional accretion in the Paleozoic and forms a broad accretionary collage tectonic belt, establishes a new working model of accretionary wedge-accretionary wedge collage complex accretionary orogeny, and points out that compound accretionary orogeny is one of the main mechanisms of hyperplasia in Central Asia continent in the Phanerozoic.
Xiao Xuchang (October 12, 1930 - December 6, 2023), born in Anshun, Guizhou, is a structural geologist, academician of the Chinese Academy of Sciences, and a researcher at the Institute of Geology, Chinese Academy of Geological Sciences.
Xiao Xuchang graduated from the Department of Geology of Peking University in 1952, and then worked in the 641 Geological Team directly under the Ministry of GeologyIn 1954, he was transferred back to Beijing by the Ministry of Geology and worked in the Nonferrous Metals Division of the Department of Geology and Mineral Resources of the Ministry of GeologyIn 1957, he followed Huang Jiqing as an academic assistantFrom 1986 to 1988, he served as the director of the Institute of Geology, Chinese Academy of Geological SciencesIn 1991, he was elected as a member (academician) of the Chinese Academy of SciencesIn 2003, he won the Ho Leung Ho Lee Science and Technology Progress Award. At 10:30 on December 6, 2023, he passed away in Beijing at the age of 94 due to ineffective medical treatment.
Xiao Xu is often mainly engaged in the study of plate tectonics and ophiolite, and participated in the evaluation of the polymetallic deposits of Xiaotieshan outside the ** plant in the 50s of the 20th centuryHe participated in the compilation of "Tectonic Map of China" and "Basic Characteristics of Geotectonic Map of China". He is engaged in the study of plate tectonics and ophiolite, and has earlier expounded the high-pressure metamorphic zone of blue schist in the Qilian Mountains and established a complete ophiolite profile in China. It is proposed that the formation and uplift of the Tibetan Plateau and its effects are uneven in time and space, and have "multi-stage, multi-level and multi-factor" control. Seven main processes of tectonic evolution in orogenic belts, from discrete to collisional orogenic formations, are divided, and ophiolite, an important symbol of orogenic belts, is dynamically classified.
Xie Shucheng, born in Longyou, Zhejiang Province in October 1967, is a geobiologist, academician of the Chinese Academy of Sciences, professor and doctoral supervisor of China University of Geosciences (Wuhan).
Xie Shucheng graduated from China University of Geosciences (Wuhan) in 1989In 1992, he obtained a master's degree from China University of Geosciences (Wuhan).In 1997, he received his Ph.D. degree from China University of Geosciences (Wuhan).From 1997 to 1998, he was engaged in postdoctoral research at the Lanzhou Institute of Glaciology and Permafrost, Chinese Academy of SciencesFrom 1999 to 2000, he was a visiting scholar at the Biogeochemistry Research Centre, Department of Chemistry, University of Bristol, UKIn 2000, he served as a professor at the School of Earth Sciences, China University of Geosciences (Wuhan).In 2005, he was awarded the National Science Grant for Distinguished Young ScholarsIn 2010, as the chief scientist, he presided over the National Key Basic Research and Development Program (973 Program).In 2014, he was selected as a leading talent in scientific and technological innovation of the Ten Thousand Talents ProgramIn 2021, he was elected as an academician of the Chinese Academy of Sciences.
Xie Shucheng has been engaged in geobiology research for a long time, focusing on geological microorganisms. Focusing on the geological problem of microorganisms in geological time, a systematic innovation chain has been formed from technical method innovation to theoretical understanding breakthrough to new discipline expansion. He innovated the instrumental analysis and data characterization methods of geological microbial lipids, and established a series of original geological microbial indicators for tracing paleoclimate and paleoenvironment. On land, he used these indicators to find that the dry and wet conditions in eastern China at different time scales over the past 8 million years have shown the spatial variation of tripolar modes. In the ocean, he found 2500 million years ago, when the worst mass extinction occurred, there were two outbreaks of some geological microorganisms. Through his innovative work on geomicrobiology, he has led to the rapid development of this new interdisciplinary discipline of geobiology in China.
Xu Guanhua, born in Shanghai on December 16, 1941, is a resource remote sensing scientist, a member of the Chinese Academy of Sciences, an academician of the Third World Academy of Sciences, a foreign academician of the Royal Swedish Academy of Engineering Sciences, an academician of the International Academy of Astronautics, a researcher and former director of the Institute of Remote Sensing and Digital Earth of the Chinese Academy of Sciences, and the former minister of science and technology.
After graduating from Beijing Forestry College in 1963, Xu Guanhua was assigned to work at the Chinese Academy of Forestry, successively serving as a research Xi, teacher, assistant researcher, researcher, and director of the Institute of Resource InformationFrom 1979 to 1981, he worked at Stockholm University, Sweden, engaged in research on remote sensing digital image processingHe joined the Communist Party of China in 1984In 1992, he was elected as a member (academician) of the Chinese Academy of SciencesIn 1993, he served as the director of the Institute of Remote Sensing Applications, Chinese Academy of SciencesFrom 1994 to 1995, he served as Vice President of the Chinese Academy of SciencesIn 1995, he served as Deputy Director of the State Science and Technology CommissionFrom 2001 to 2007, he served as Minister of Science and Technology.
Guanhua Xu is mainly engaged in the research of resource remote sensing and geographic information system. In the research of satellite digital image processing, he has developed theories and technologies such as boundary decision-making, training sample plot analysis, image classification, patch synthesis, biomass estimation, etc., successfully developed China's earliest remote sensing satellite digital image processing system, developed the theory and method of remote sensing comprehensive survey and series of mapping, and led the compilation of the first comprehensive survey and series of mapping technical regulations for remote sensing of renewable resources, and has pioneered and creatively led the "Three Norths" in classification system, mapping scale, technical process, thematic map types, etc The comprehensive survey of remote sensing in shelterbelts has made breakthroughs in the application scale, technical difficulty and time requirements of space remote sensing.
Xu Yigang, born on October 19, 1966 in Changshu, Jiangsu, is a petrist, academician of the Chinese Academy of Sciences, researcher, doctoral supervisor and director of the Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, and director of the State Key Laboratory of Isotope Geochemistry.
Yigang Xu graduated from Zhejiang University in 1987 and received his Ph.D. from the University of Paris VII in 1994In 1995, he returned to China and joined the Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, where he served as an associate researcher and a researcherIn 1999, he was awarded the National Science Grant for Outstanding Young ScholarsIn 2004, he was selected as one of the first batch of national candidates for the New Century Millions of Talents ProjectIn 2010, he served as the director of the Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, and in the same year, he served as the director of the State Key Laboratory of Isotope GeochemistryIn 2017, he was elected as an academician of the Chinese Academy of Sciences.
Xu Yigang is mainly engaged in mantle petrology research. The main achievements include systematically summarizing the geological, petrological and geochemical evidence of lithospheric thinning in eastern China, and defining the time and mechanism of lithospheric thinning. (2) A new method for identifying ancient mantle plumes is proposed, which systematically elucidates the genesis of mantle plumes in the Great Igneous Province of Mount Emei, and provides a model for the study of the systematic behavior of different layers of the solid earth under the influence of mantle plumes. (3) It is determined that the source area of Cenozoic intraplate basalt in the East Asian continent is generally subducted in the western Pacific subduction plate, and it is proposed that the subduction component may be in the deep carbonated mantle modified by the melt of the mantle transition zone, and a new mechanism for the formation of intraplate basalt in the mantle wedge system is constructed.
Xu Zhiqin, female, born in Shanghai on August 14, 1941, is a structural geologist, academician of the Chinese Academy of Sciences, academician of the Academy of Sciences for Developing Countries, researcher and doctoral supervisor of the Institute of Geology of the Chinese Academy of Geological Sciences.
Xu Zhiqin graduated from the Department of Geology and Geography of Peking University in 1964 and was assigned to work at the Institute of Geology, Chinese Academy of Geological SciencesHe received his Ph.D. in Structural Geology from the University of Montpellier, France in 1987From 1993 to 2001, he served as Vice President of the Chinese Academy of Geological Sciences and Director of the Institute of Geology, Chinese Academy of Geological SciencesIn 1995, he was elected as an academician of the Chinese Academy of SciencesIn 1997, he served as the first director of the Open Experimental Laboratory of Continental DynamicsIn 2007, he was elected as a member of the Academy of Sciences for the Developing World (TWAS).In 2016, he served as the chief engineer of the China Geological Survey.
Xu Zhiqin is mainly engaged in the study of rift structure, deformation structure, orogeny and orogenic mechanism of the Qinghai-Tibet Plateau and the surrounding orogenic belt. Firstly, the geometry, kinematics, dynamics and quantitative analysis of structural geology were applied to the study of the Qinghai-Tibet Plateau and the Chinese orogenic belt, and more than 50 large-scale ductile shear zones in China were determined, which laid the foundation for the research of the deformation tectonic system of several orogenic belts in the western region, and the ultra-high pressure quartz minerals in the Dabie Mountains were discovered for the first time in 1987, and a series of important ideas and theories were put forward in the collision dynamics and orogenic mechanism of the Qinghai-Tibet Plateau. The first to implement the "Continental Dynamics" program in China. The scientific drilling project in Chinese mainland was completed in 2005 and has had a significant impact both inside and outside China.
Yang Jingsui, born in June 1950 in Hangzhou, Zhejiang, is a rock tectonist, an academician of the Chinese Academy of Sciences, and a researcher of the Institute of Geology, Chinese Academy of Geological Sciences.
Yang Jingsui graduated from Changchun Institute of Geology in 1977He received his Ph.D. from Dalhousie University in 1992In 1995, he was appointed as a researcher at the Institute of Geology, Chinese Academy of Geological SciencesIn 1997, he was appointed as the director of the Igneous Rock Laboratory of the Institute of Geology, Chinese Academy of Geological Sciences, and the director of the Key Laboratory of Continental Dynamics of the Ministry of Land and ResourcesFrom 1998 to 2000, he served as the deputy director of the Institute of Geology, Chinese Academy of Geological SciencesIn 2017, he was elected as an academician of the Chinese Academy of Sciences.
Yang Jingsui is mainly engaged in the research and teaching of petrology and tectonics of the Qinghai-Tibet Plateau and orogenic belts. In-situ diamond was found in ophiolite chromite and proved to be a new type of production in nature, named "ophiolite type diamond";A large number of ultra-high pressure and strongly reducing mineral assemblages have been found in the ophiolite of multiple plate suture zones around the world, and the deep mantle cycle of subducted materials and the deep genesis model of chromite have been established, which has opened an important new window for the study of deep mantle materialsThree high-pressure and ultra-high-pressure metamorphic belts were discovered and determined, including the northern margin of Chai, the East Qinling Mountains and the Songduo of ChinaDetermination of the Paleozoic ophiolite assembles of the East Kunlun Animaqing and West Kunlun reservoirs.
Yang Shufeng, born in Hangzhou, Zhejiang Province in May 1947, is a structural geologist, academician of the Chinese Academy of Sciences, professor and doctoral supervisor of the School of Earth Sciences of Zhejiang University, and director of the Research Center for Oil and Gas Basin Tectonics of the Ministry of Education.
In 1975, Yang Shufeng graduated from the Department of Geology, Nanjing University, majoring in mineralogyHe received a master's degree from Nanjing University in 1981He received his Ph.D. from Nanjing University in 1984, the first Ph.D. in geology in ChinaIn 1989, he was appointed as the head of the Department of Earth Sciences, Zhejiang UniversityIn 2004, he was awarded the National Model TeacherIn 2008, he was selected as a special expert in Zhejiang ProvinceIn 2011, he won the Zhu Kezhen Award of Zhejiang UniversityIn 2013, he was awarded the honorary title of Meritorious Teacher of Zhejiang ProvinceIn 2015, he was elected as an academician of the Chinese Academy of Sciences.
Yang Shufeng is mainly engaged in the research and education of structural geology, and his research areas are geotectonics, orogenic belts and basin tectonics. He proposed the concept of "paired granite belts", which revealed the change law of physical properties of different types of granite under high temperature and high pressure, and enriched the theory of granite genesisThe Tarim Great Igneous Province was discovered, and the relationship between the Great Igneous Province and the tectonic evolution of Tethys was proposed, which enriched the theory of the genesis of the Great Igneous ProvinceThe tectonic deformation characteristics and oil and gas control laws of the thrust belt in western China under the control of the long-distance effect of plate collisions are proposed, which provides theoretical support for the search for oil and gas under the Early Paleozoic overburden in western China, and is confirmed by exploration.
List of Quality Authors (To be continued).